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안영길(Ahn, Young Gil),조명숙(Cho, Myoung Suk) 한국유아교육·보육복지학회 2016 유아교육·보육복지연구 Vol.20 No.4
본 연구는 그림책 읽기 과정에서 일어나는 유아독자의 이해방식을 알아보고 효과적인 읽기방법을 제시하는데 목적이 있다. 이를 위해 그림책 속 이야기를 구조적 분석의 대상으로 보는 기호학적 관점, 반성적 철학의 틀 속에서 존재론적 시선으로 보는 해석학적 관점으로 이해방식을 각각 살펴보았다. 먼저, 유아는 그림책이란 텍스트를 읽고 그 속에 담긴 의미를 구성하기 위해 상징 그 자체가 어떤 구조와 의미로 이루어져 있는지, 어떻게 의미를 생성하고 해석되어지는가를 분석하는 기호학적 관점에서의 이해가 필요하다. 더불어 유아독자의 배경지식과 경험을 바탕으로 심적 변화에 궁극적인 목적이 있는 해석학적 이해도 반드시 수반되어야 한다. 따라서 기호학과 해석학의 이론적 관점에 따라 다음과 같은 그림책 읽기 방법을 제안 한다. 첫째, 유아의 배경지식 및 상호텍스트성을 활용한 그림책 읽기, 둘째, 그림책의 파라텍스트 요소와 그림을 활용한 훑어보며 읽기, 셋째, 그림책의 글 텍스트와 그림 텍스트를 연결 지으며 읽기, 넷째, 그림책 읽기과정에서 최대한 자유로운 분위기를 조성하여 유아의 생생하고 자유로운 반응을 격려하며 읽기, 다섯째, 반복적 그림책 읽기 활동을 적극적으로 권장하며 읽기를 제안하였다. The purpose of this study is to examine the comprehension method of readers occurring during the process of reading picture book and present effective reading methods. Accordingly, comprehension method was examined respectively through a semiotic perspective that looks at a story in picture book as a subject of structural analysis, and a hermeneutics perspective of looking at it from an ontological view within a framework of reflective philosophy. First off, readers need an understanding from a semiotic perspective of reading the text of picture book to analyze its structure with symbolism to compose meaning within, as well as its meaning and the process of creating and interpreting such meaning. Furthermore, they also require an understanding from a hermeneutics perspective with the ultimate goal in psychological change based on their background knowledge and experiences. Accordingly, following methods of reading picture book are proposed. First, picture book reading using readers’ background knowledge and intertextuality. Second, glance reading using picture book’s para-text element and picture. Third, reading by connecting between picture book’s written text and picture text. Fourth, reading by encouraging children’s vivid and free response by forming a free atmosphere as much as possible during picture book reading process. Fifth, reading by actively recommending repetitive picture book reading activity.
김영택(Young-Taeg Kim),김주연(Joo-youn Kim),안영길(Young-Gil Ahn),한정식(Jung-Sik Han),김호균(Ho Kyun Kim),이은일(Eun-Il Lee) 한국항해항만학회 2008 한국항해항만학회 학술대회논문집 Vol.2008 No.공동학술
Corrections for multibeam soundings were reviewed to improve the method for tide correction. There are four correction methods for navigation, sounding, error, and tide. Among them, tide correction method was mainly investigated. Currently, four tide correction methods, such as constants for correction (time difference and height ratio for tide) and numerical tidal model are reviewed to identify the strengths and weakness of each method, and corresponding improving ways. They need to be carefully examined to identify advantages and disadvantages for the hybrid method to correct tide.
김영택(Young-Taeg Kim),김주연(Joo-youn Kim),안영길(Young-Gil Ahn),한정식(Jung-Sik Han),김호균(Ho Kyun Kim),이은일(Eun-Il Lee) 한국마린엔지니어링학회 2008 한국마린엔지니어링학회 학술대회 논문집 Vol.2008 No.-
Corrections for multibeam soundings were reviewed to improve the method for tide correction. There are four correction methods for navigation, sounding, error, and tide. Among them, tide correction method was mainly investigated. Currently, four tide correction methods, such as constants for correction (time difference and height ratio for tide) and numerical tidal model are reviewed to identify the strengths and weakness of each method, and corresponding improving ways. They need to be carefully examined to identify advantages and disadvantages for the hybrid method to correct tide.
한반도 서해연안에 분포하는 사질퇴적체의 분포 및 음향특성연구
한혁수(Hyuk-Soo Han),이상민(Sang-Min Lee),정초기(Cho-Ki Jung),안영길(Young-Gil Ahn),김서철(Seo-Cheal Kim),박인영(In-Young Park) 한국마린엔지니어링학회 2009 한국마린엔지니어링학회 학술대회 논문집 Vol.2009 No.-
A Large part of the sea floor in the western shelf of Korea peninsula is covered by sand deposits witch formed during the postglacial transgression(Park et al. 2006). Distribute echo character of shelf sand ridge into four classes (Type Ⅰ, Type Ⅱ, Type Ⅲ, Type Ⅳ). These shelf sand ridges are large and elongate shape with a length up to 100 ㎞ and width 1 to 10 ㎞.